摘要
文章根据铀储集层及其地下水地质演化历史,推断控矿的层间氧化带发育程度,分析铀矿床仅在3条较大河流两侧形成的原因,总结了与铀成矿配套的水文地质条件,为类似地区铀矿找矿工作提供了理论依据。
Based on the evolution of uranium storage layer and the groundwater,the author first deduced the development degree of ore-controlling interlayer oxidized zones,analyzed the reason of the deposits location by the side of the three major rivers,then summarized the hydro-geological condition for uranium mineralization and finaly made the theory basis for uranium prospecting in similar region.
出处
《铀矿地质》
CAS
CSCD
2011年第4期225-230,共6页
Uranium Geology
关键词
伊犁盆地南缘
地下水演化
铀源
southern margin of Yili basin
groundwater development
uranium resources
